东昆仑造山带具有软碰撞、多旋回的特点，造山带内的沉积盆地具有多物源和不同的大地构造背景。
The eastern Kunlun orogenic belt shows characteristics of soft-collision and multi-cycles. The sedimentary basins inside it have multi-sources and different tectonic backgrounds.
软沉积物变形构造是确定古地震存在的关键证据之一。
Soft sediment deformation is one of the key indicators identifying the existence of paleo-earthquake.
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